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Biver, M., Shotyk, W. (2013) Stibiconite (Sb3O6OH), senarmontite (Sb2O3) and valentinite (Sb2O3): Dissolution rates at pH 2–11 and isoelectric points. Geochimica et Cosmochimica Acta, 109. 268-279 doi:10.1016/j.gca.2013.01.033

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Reference TypeJournal (article/letter/editorial)
TitleStibiconite (Sb3O6OH), senarmontite (Sb2O3) and valentinite (Sb2O3): Dissolution rates at pH 2–11 and isoelectric points
JournalGeochimica et Cosmochimica Acta
AuthorsBiver, M.Author
Shotyk, W.Author
Year2013 (May)Volume109
PublisherElsevier BV
DOIdoi:10.1016/j.gca.2013.01.033Search in ResearchGate
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Mindat Ref. ID355299Long-form Identifiermindat:1:5:355299:9
GUID0
Full ReferenceBiver, M., Shotyk, W. (2013) Stibiconite (Sb3O6OH), senarmontite (Sb2O3) and valentinite (Sb2O3): Dissolution rates at pH 2–11 and isoelectric points. Geochimica et Cosmochimica Acta, 109. 268-279 doi:10.1016/j.gca.2013.01.033
Plain TextBiver, M., Shotyk, W. (2013) Stibiconite (Sb3O6OH), senarmontite (Sb2O3) and valentinite (Sb2O3): Dissolution rates at pH 2–11 and isoelectric points. Geochimica et Cosmochimica Acta, 109. 268-279 doi:10.1016/j.gca.2013.01.033
In(2013) Geochimica et Cosmochimica Acta Vol. 109. Elsevier BV

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Biver, M., & Shotyk, W. (2013). Stibiconite (Sb 3 O 6 OH), senarmontite (Sb 2 O 3) and valentinite (Sb 2 O 3): Dissolution rates at pH 2–11 and isoelectric points. Geochimica et Cosmochimica Acta, 109, 268-279.
Biver, Marc, Shotyk, William (2012) Stibnite (Sb2S3) oxidative dissolution kinetics from pH 1 to 11. Geochimica et Cosmochimica Acta, 79. 127-139 doi:10.1016/j.gca.2011.11.033
Zhang, Youxue (2006) Quantifying mineral dissolution and xenolith digestion rates. Geochimica et Cosmochimica Acta, 70 (18) doi:10.1016/j.gca.2006.06.1327
Marieni, Chiara, Voigt, Martin J., Oelkers, Eric H. (2021) Experimental study of epidote dissolution rates from pH 2 to 11 and temperatures from 25 to 200 °C. Geochimica et Cosmochimica Acta, 294. 70-88 doi:10.1016/j.gca.2020.11.015
Yang, Li, Steefel, Carl I. (2008) Kaolinite dissolution and precipitation kinetics at 22°C and pH 4. Geochimica et Cosmochimica Acta, 72 (1) 99-116 doi:10.1016/j.gca.2007.10.011
Fenter, Paul, Zapol, Peter, He, Haiying, Sturchio, Neil C. (2014) On the variation of dissolution rates at the orthoclase (0 0 1) surface with pH and temperature. Geochimica et Cosmochimica Acta, 141. 598-611 doi:10.1016/j.gca.2014.06.019
Olsen, Amanda Albright, Donald Rimstidt, J. (2008) Oxalate-promoted forsterite dissolution at low pH. Geochimica et Cosmochimica Acta, 72 (7) 1758-1766 doi:10.1016/j.gca.2007.12.026
Salehikhoo, Fatemeh, Li, Li, Brantley, Susan L. (2013) Magnesite dissolution rates at different spatial scales: The role of mineral spatial distribution and flow velocity. Geochimica et Cosmochimica Acta, 108. 91-106 doi:10.1016/j.gca.2013.01.010
Boudreau, Bernard P., Sulpis, Olivier, Mucci, Alfonso (2020) Control of CaCO3 dissolution at the deep seafloor and its consequences. Geochimica et Cosmochimica Acta, 268. 90-106 doi:10.1016/j.gca.2019.09.037
Wolff-Boenisch, Domenik, Gislason, Sigurdur R., Oelkers, Eric H. (2004) The effect of fluoride on the dissolution rates of natural glasses at pH 4 and 25°C. Geochimica et Cosmochimica Acta, 68 (22) 4571-4582 doi:10.1016/j.gca.2004.05.026
Mulders, Josephina J.P.A., Oelkers, Eric. H. (2020) An experimental study of sepiolite dissolution rates and mechanisms at 25 °C. Geochimica et Cosmochimica Acta, 270. 296-312 doi:10.1016/j.gca.2019.11.026
 
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